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. 2018 Oct 30;8:16001. doi: 10.1038/s41598-018-34450-3

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© The Author(s) 2018

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

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Projected Arctic rainfall changes attributed to changes in local temperature, for annual mean (top), summer (JJA, June-July-August; bottom left) and winter (DJF, December-January-February; bottom right). 100% percent means that the increase in rainfall can be totally attributed to local warming. Yellow dots in the top panel show the locations (one on the North Pole and one in the North Atlantic) used in Fig. 4.